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Biermann Quarries (Bethel quarries; Codfish Hill Quarry), Bethel, Fairfield County, Connecticut, USAi
Regional Level Types
Biermann Quarries (Bethel quarries; Codfish Hill Quarry)Quarry (Abandoned)
Bethel- not defined -
Fairfield CountyCounty
ConnecticutState
USACountry

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PhotosMapsSearch
02535960017272023876344.jpg
Collecting on the dumps at Bierman Quarry 1979

Biermann Quarries, Bethel, Fairfield County, Connecticut, USA
00101890017272023888020.jpg
Elmore Easter collecting on the dumps at Bierman Quarry

Biermann Quarries, Bethel, Fairfield County, Connecticut, USA
02535960017272023876344.jpg
Collecting on the dumps at Bierman Quarry 1979

Biermann Quarries, Bethel, Fairfield County, Connecticut, USA
00101890017272023888020.jpg
Elmore Easter collecting on the dumps at Bierman Quarry

Biermann Quarries, Bethel, Fairfield County, Connecticut, USA
Latitude & Longitude (WGS84):
41° 21' 15'' North , 73° 21' 2'' West
Latitude & Longitude (decimal):
Type:
Quarry (Abandoned) - last checked 2023
Kรถppen climate type:
Nearest Settlements:
PlacePopulationDistance
Bethel9,549 (2017)5.6km
Newtown1,967 (2017)7.7km
Danbury84,657 (2017)9.7km
Easton7,625 (2017)12.1km
Georgetown1,805 (2017)13.0km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Danbury Mineralogical SocietyDanbury, Connecticut10km
New Haven Mineral ClubNew Haven, Connecticut36km
Stamford Mineralogical SocietyStamford, Connecticut37km
Bristol Gem & Mineral ClubBristol, Connecticut49km
Lapidary and Mineral Society of Central ConnecticutMeriden, Connecticut50km
Mindat Locality ID:
6788
Long-form identifier:
mindat:1:2:6788:4
GUID (UUID V4):
0


Two adjacent quarries in a granite pegmatite now well-known for its bertrandite crystals. Most references describe or list minerals but provide little history. Todd (1906) visited the "recently opened" quarry and reported that "This vein, we learned, is controlled jointly by the New Jersey Flint and Spar Company and the International Pottery, both of Trenton, New Jersey, and all its stone is shipped there." He mentions an immense tourmaline crystal measuring 3 feet by 18 inches that had been taken from the workings. The quarry apparently was not active during WWII because it does not appear in Cameron et al's (1954) Pegmatite Investigations 1942-45 New England. It may have been worked for beryl in the 1950s. Hiller (1982) claims it was worked in the 19th century for mica and in the early 20th century for mica and feldspar. He collected there after 1965 into the 1980s. It is located in Huntington State Park.

Some references such as Schooner (1961) refer to this quarry incorrectly as the Codfish Hill Quarry, though the minerals he describes are correct for Biermann.

This internally zoned pegmatite has small vugs and pockets in the albite-rich zone containing generally microcrystals of albite, muscovite, fluorapatite (white to pale blue), quartz, beryl (rarely), and lesser quantities of unusual (for a pegmatite) lead minerals like wulfenite, cerrusite and pyromorphite described by Januzzi (1959). Bertrandite microcrystals described by Hiller (1982) and Henderson (1975, 1995) made this pegmatite well-known among collectors. Many beryl crystals here are pseudomorphed by a dull-brown, fine-grained mixture of bertrandite, muscovite, adularia, quartz and albite.

Nearby tourmaline-rich ledges have a separate locality page:
https://www.mindat.org/loc-457625.html
Please post minerals from there to that mindat page.

NOTE: Into the 1980s, collecting permission could be obtained from the park ranger (Hiller, 1982). However, it is no longer allowed. All mineral collecting in Collis P. Huntington State Park is illegal and will be prosecuted.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


24 valid minerals. 1 erroneous literature entry.

Detailed Mineral List:

โ“˜ Acanthite ?
Formula: Ag2S
Habit: massive
Colour: black
Description: Microscopic black masses with post-collecting crystal overgrowths.
โ“˜ Albite
Formula: Na(AlSi3O8)
Habit: massive, tabular, blocky angular overgrowths
Colour: white
Description: Vast majority is massive primary pegmatite constituent. Secondary crystals occur as micro-overgrowths on walls of small voids and as part of a suite of micro-minerals pseudomorphing beryl.
โ“˜ Almandine
Formula: Fe2+3Al2(SiO4)3
Habit: trapezohedral
Colour: maroon
Description: Massive material, commonly with blue-green to white fluorapatite.
โ“˜ Annite
Formula: KFe2+3(AlSi3O10)(OH)2
Colour: black
Description: minor accessory mineral
โœช Bertrandite
Formula: Be4(Si2O7)(OH)2
Habit: multiple forms, from simple to complex and as various twins. Usually flattened, elongated, or blocky.
Colour: colorless
Description: Micro-crystals and aggregates in voids left by dissolved beryl crystals. Also part of a suite of micro-minerals pseudomorphing beryl crystals.
โ“˜ Beryl
Formula: Be3Al2(Si6O18)
Habit: Hexagonal prisms elongated along c axis. Commonly tapered.
Colour: orange-yellow, pale yellow to pale green, brown when altered
Description: Crystals can be large (over 60 cm), though typically subhedral, and multi-colored, and varying from partly gemmy to brown, opaque, and altered to a fine-grained mixture of bertrandite, muscovite, adularia, quartz and albite. Many crystals are found frozen in matrix in a subparallel arrangement with one end rooted in a layer mica.
โ“˜ Bismutite
Formula: (BiO)2CO3
Habit: earthy, as pseudomorphs after bismuthinite
Colour: gray
Description: earthy gray pseudomorphs after elongated, striated bismuthinite crystals up to a few cms.
โ“˜ Cerussite
Formula: PbCO3
Habit: equant, dipyramidal, pseudo-hexagonal
Colour: Yellowish white
Description: In addition to free-growing crystals, the cerussite is also found as megascopic and microscopic crystalline masses and grains associated with wulfenite and pyromorphite.
โ“˜ 'Chlorite Group'
Habit: massive and micaceous in the schist, pseudohexagonal in the pegmatite
Colour: dark green in the schist, in the pegmatite as zoned nearly black interior and white exterior.
Description: Abundant in the schist near the pegmatite. Also very rarely as tiny crystals and crusts in voids in the pegmatite.
โœช 'Columbite-(Fe)-Columbite-(Mn) Series'
Habit: flat, elongated prisms or subhedral masses
Colour: black, with iridescence
Description: Good prismatic crystals formed in quartz, also hand-sized subhedral masses with striations from neighboring muscovite. Januzzi (1976) reports that a beryl crystal with a large columbite crystal projecting from it was donated to the American Museum of Natural History in New York City. The ID is generic, at least one crystal was tested using Raman spectroscopy and the best match is tantalite-(Fe) (see entry). A crystal formerly in the Bill Shelton collection has a specific gravity of 6.7, making it clearly a columbite species.
โ“˜ 'Cymatolite' ?
Description: The complete absence of spodumene at Biermann makes the occurence of cymatolite here hightly unlikely. Quite possibly the reported find was a cymatolite found at the Fillow Quarry (not too far away) and discard by a collector at Biermann.
โ“˜ 'Fergusonite' ?
Colour: brownish yellow
Description: reported by Januzzi (1976) as "a small, brownish yellow nodule in feldspar". No analysis reported, no other finds reported/confirmed.
โ“˜ Fluorapatite
Formula: Ca5(PO4)3F
Habit: massive to subhedral tabular
Colour: white to blue-green
Fluorescence: yellow under SW UV
Description: Typically massive and associated with maroon almandine. Color can vary between white and blue-green in the same chunk, with bright yellow SW UV fluorescence only from the white zones.
โ“˜ 'Gummite'
Description: Apparently an alteration of uraninite.
โ“˜ Hematite
Formula: Fe2O3
โ“˜ 'K Feldspar'
Colour: white
Description: See comments for adularia variety.
โ“˜ 'K Feldspar var. Adularia'
Formula: KAlSi3O8
Habit: rectangular with acute pinacoids to flat pseudo-rhombohedral
Colour: white to pale pink
Description: Part of a suite of microminerals pseudomorphing beryl: bertrandite, muscovite, albite, quartz.
โ“˜ Meta-autunite
Formula: Ca(UO2)2(PO4)2 · 6H2O
Habit: square tabular
Colour: yellow-green
Fluorescence: bright green under SW UV
Description: Secondary microcrystals from the alteration of primary uraninite.
โ“˜ Microcline
Formula: K(AlSi3O8)
Colour: white to tan
Description: Primary constituent of the pegmatite matrix, crystals rare and typically subhedral.
โ“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Habit: tabular subhedral
Colour: silvery to pale olive green
Description: Major accessory pegmatite mineral, in books up to several 10s of cm, pseudmorphing schorl, or as part of a suite of microminerals pseudomorphing beryl: bertrandite, adularia, albite, quartz.
โ“˜ Opal
Formula: SiO2 · nH2O
Habit: coatings
Colour: colorless
Fluorescence: bright green under SW UV
Description: Minor coatings on fracture surfaces, nearly impossible to see without using a UV lamp.
โ“˜ Opal var. Opal-AN
Formula: SiO2 · nH2O
Habit: coatings
Colour: colorless
Fluorescence: bright green under SW UV
Description: Minor coatings on fracture surfaces, nearly impossible to see without using a UV lamp.
โ“˜ Pyrite
Formula: FeS2
โ“˜ Pyrolusite
Formula: Mn4+O2
Description: No pyrolusite dendrite or staining in the world has been verified as pyrolusite. The name was a mistake in the nineteenth century which has been widely publicized.
โ“˜ Pyromorphite
Formula: Pb5(PO4)3Cl
Habit: micro-encrustations
Colour: yellow-green
Description: Associated with microcrystals of wulfenite and cerussite in vuggy albite.
โ“˜ Quartz
Formula: SiO2
Habit: elongated prismatic
Colour: smoky to milky
Description: The vast majority of material is a massive primary constituent of the pegmatite matrix. Small to microcrystals are secondary overgrowths lining small void or as part of a suite of microminerals pseudomorphing beryl: bertrandite, adularia, albite, muscovite.
โ“˜ Schorl
Formula: NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
Habit: elongated trigonal prismatic
Colour: black
Description: An accessory mineral in the pegmatite, crystals up to 3 feet long and commonly tapered along their long axis. Many are partly or completely altered to muscovite.
โ“˜ Spessartine
Formula: Mn2+3Al2(SiO4)3
Habit: massive
Colour: red
Description: Massive material associated with blue-green fluorapatite in cleavelandite.
โ“˜ Tantalite-(Fe)
Formula: Fe2+Ta2O6
Description: At least one "columbite" from here was tested using Raman spectroscopy at the University of New Haven and best match is tantalite-(Fe).
โ“˜ Uraninite
Formula: UO2
Habit: octahedral
Colour: black
Description: Crystals typically small and subhedral.
โ“˜ Uranophane
Formula: Ca(UO2)2(SiO3OH)2 · 5H2O
Description: Alteration of uraninite.
โ“˜ Wulfenite
Formula: Pb(MoO4)
Habit: tabular, elongated prismatic bipyramidal
Colour: orange
Description: Microcrystals associated with equally small cerussite and pyromorphite crystals in vuggy albite.
โ“˜ Zircon
Formula: Zr(SiO4)
โ“˜ Zircon var. Cyrtolite
Formula: Zr[(SiO4),(OH)4]
Habit: branching aggregates of prismatic crystals terminated by pyramids
Colour: brown

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
โ“˜Acanthite ?2.BA.35Ag2S
โ“˜Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
โ“˜Hematite4.CB.05Fe2O3
โ“˜Quartz4.DA.05SiO2
โ“˜Opal
var. Opal-AN
4.DA.10SiO2 ยท nH2O
โ“˜4.DA.10SiO2 ยท nH2O
โ“˜Pyrolusite ?4.DB.05Mn4+O2
โ“˜Tantalite-(Fe)4.DB.35Fe2+Ta2O6
โ“˜Uraninite4.DL.05UO2
Group 5 - Nitrates and Carbonates
โ“˜Cerussite5.AB.15PbCO3
โ“˜Bismutite5.BE.25(BiO)2CO3
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
โ“˜Wulfenite7.GA.05Pb(MoO4)
Group 8 - Phosphates, Arsenates and Vanadates
โ“˜Fluorapatite8.BN.05Ca5(PO4)3F
โ“˜Pyromorphite8.BN.05Pb5(PO4)3Cl
โ“˜Meta-autunite8.EB.10Ca(UO2)2(PO4)2 ยท 6H2O
Group 9 - Silicates
โ“˜Almandine9.AD.25Fe2+3Al2(SiO4)3
โ“˜Spessartine9.AD.25Mn2+3Al2(SiO4)3
โ“˜Zircon9.AD.30Zr(SiO4)
โ“˜var. Cyrtolite9.AD.30Zr[(SiO4),(OH)4]
โ“˜Uranophane9.AK.15Ca(UO2)2(SiO3OH)2 ยท 5H2O
โ“˜Bertrandite9.BD.05Be4(Si2O7)(OH)2
โ“˜Beryl9.CJ.05Be3Al2(Si6O18)
โ“˜Schorl9.CK.05NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
โ“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
โ“˜Annite9.EC.20KFe2+3(AlSi3O10)(OH)2
โ“˜Microcline9.FA.30K(AlSi3O8)
โ“˜Albite9.FA.35Na(AlSi3O8)
Unclassified
โ“˜'K Feldspar
var. Adularia'
-KAlSi3O8
โ“˜'Chlorite Group'-
โ“˜'Gummite'-
โ“˜'Cymatolite' ?-
โ“˜'Columbite-(Fe)-Columbite-(Mn) Series'-
โ“˜'K Feldspar'-
โ“˜'Fergusonite' ?-

List of minerals for each chemical element

HHydrogen
Hโ“˜ AnniteKFe32+(AlSi3O10)(OH)2
Hโ“˜ BertranditeBe4(Si2O7)(OH)2
Hโ“˜ Opal var. Opal-ANSiO2 · nH2O
Hโ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Hโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hโ“˜ OpalSiO2 · nH2O
Hโ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Hโ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Hโ“˜ Zircon var. CyrtoliteZr[(SiO4),(OH)4]
BeBeryllium
Beโ“˜ BertranditeBe4(Si2O7)(OH)2
Beโ“˜ BerylBe3Al2(Si6O18)
BBoron
Bโ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
CCarbon
Cโ“˜ Bismutite(BiO)2CO3
Cโ“˜ CerussitePbCO3
OOxygen
Oโ“˜ K Feldspar var. AdulariaKAlSi3O8
Oโ“˜ AlbiteNa(AlSi3O8)
Oโ“˜ AnniteKFe32+(AlSi3O10)(OH)2
Oโ“˜ AlmandineFe32+Al2(SiO4)3
Oโ“˜ BertranditeBe4(Si2O7)(OH)2
Oโ“˜ Bismutite(BiO)2CO3
Oโ“˜ BerylBe3Al2(Si6O18)
Oโ“˜ CerussitePbCO3
Oโ“˜ Tantalite-(Fe)Fe2+Ta2O6
Oโ“˜ FluorapatiteCa5(PO4)3F
Oโ“˜ HematiteFe2O3
Oโ“˜ Opal var. Opal-ANSiO2 · nH2O
Oโ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Oโ“˜ MicroclineK(AlSi3O8)
Oโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oโ“˜ OpalSiO2 · nH2O
Oโ“˜ PyrolusiteMn4+O2
Oโ“˜ PyromorphitePb5(PO4)3Cl
Oโ“˜ QuartzSiO2
Oโ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Oโ“˜ SpessartineMn32+Al2(SiO4)3
Oโ“˜ UraniniteUO2
Oโ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Oโ“˜ WulfenitePb(MoO4)
Oโ“˜ ZirconZr(SiO4)
Oโ“˜ Zircon var. CyrtoliteZr[(SiO4),(OH)4]
Oโ“˜ Columbite-(Fe)-Columbite-(Mn) Series
FFluorine
Fโ“˜ FluorapatiteCa5(PO4)3F
NaSodium
Naโ“˜ AlbiteNa(AlSi3O8)
Naโ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
AlAluminium
Alโ“˜ K Feldspar var. AdulariaKAlSi3O8
Alโ“˜ AlbiteNa(AlSi3O8)
Alโ“˜ AnniteKFe32+(AlSi3O10)(OH)2
Alโ“˜ AlmandineFe32+Al2(SiO4)3
Alโ“˜ BerylBe3Al2(Si6O18)
Alโ“˜ MicroclineK(AlSi3O8)
Alโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alโ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Alโ“˜ SpessartineMn32+Al2(SiO4)3
SiSilicon
Siโ“˜ K Feldspar var. AdulariaKAlSi3O8
Siโ“˜ AlbiteNa(AlSi3O8)
Siโ“˜ AnniteKFe32+(AlSi3O10)(OH)2
Siโ“˜ AlmandineFe32+Al2(SiO4)3
Siโ“˜ BertranditeBe4(Si2O7)(OH)2
Siโ“˜ BerylBe3Al2(Si6O18)
Siโ“˜ Opal var. Opal-ANSiO2 · nH2O
Siโ“˜ MicroclineK(AlSi3O8)
Siโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siโ“˜ OpalSiO2 · nH2O
Siโ“˜ QuartzSiO2
Siโ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Siโ“˜ SpessartineMn32+Al2(SiO4)3
Siโ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Siโ“˜ ZirconZr(SiO4)
Siโ“˜ Zircon var. CyrtoliteZr[(SiO4),(OH)4]
PPhosphorus
Pโ“˜ FluorapatiteCa5(PO4)3F
Pโ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Pโ“˜ PyromorphitePb5(PO4)3Cl
SSulfur
Sโ“˜ AcanthiteAg2S
Sโ“˜ PyriteFeS2
ClChlorine
Clโ“˜ PyromorphitePb5(PO4)3Cl
KPotassium
Kโ“˜ K Feldspar var. AdulariaKAlSi3O8
Kโ“˜ AnniteKFe32+(AlSi3O10)(OH)2
Kโ“˜ MicroclineK(AlSi3O8)
Kโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
CaCalcium
Caโ“˜ FluorapatiteCa5(PO4)3F
Caโ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Caโ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
MnManganese
Mnโ“˜ PyrolusiteMn4+O2
Mnโ“˜ SpessartineMn32+Al2(SiO4)3
Mnโ“˜ Columbite-(Fe)-Columbite-(Mn) Series
FeIron
Feโ“˜ AnniteKFe32+(AlSi3O10)(OH)2
Feโ“˜ AlmandineFe32+Al2(SiO4)3
Feโ“˜ Tantalite-(Fe)Fe2+Ta2O6
Feโ“˜ HematiteFe2O3
Feโ“˜ PyriteFeS2
Feโ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Feโ“˜ Columbite-(Fe)-Columbite-(Mn) Series
ZrZirconium
Zrโ“˜ ZirconZr(SiO4)
Zrโ“˜ Zircon var. CyrtoliteZr[(SiO4),(OH)4]
NbNiobium
Nbโ“˜ Columbite-(Fe)-Columbite-(Mn) Series
MoMolybdenum
Moโ“˜ WulfenitePb(MoO4)
AgSilver
Agโ“˜ AcanthiteAg2S
TaTantalum
Taโ“˜ Tantalite-(Fe)Fe2+Ta2O6
PbLead
Pbโ“˜ CerussitePbCO3
Pbโ“˜ PyromorphitePb5(PO4)3Cl
Pbโ“˜ WulfenitePb(MoO4)
BiBismuth
Biโ“˜ Bismutite(BiO)2CO3
UUranium
Uโ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Uโ“˜ UraniniteUO2
Uโ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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